Drilling at the Kebigada deposit has confirmed the “main zone” mineralisation exists over 1.3km to 1.5km with widths of up to 350-400m and depths exceeding 300m. Mineralisation is strongly associated with silica flooding, quartz stringers and sulphides (pyrite and chalcopyrite). High grade mineralisation (>3g/t Au) is associated with east-west trending quartz stringers and pyrite/chalcopyrite laminae. Mineralisation has an apparent plunge to the north which highlights the underground potential. Amani gold states they now expect to complete a Feasibility Study at the beginning of 2020.
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